Modelagem Radiativa-Condutiva do Fluxo de Radiação que Atravessa a Atmosfera Terrestre com uma Camada de Nuvens
O objetivo desse trabalho é estimar o fluxo de radiação que atravessa a atmosfera terrestre com uma camada de nuvens por meio de uma modelagem radiativo-condutiva, usando um método composto pela transformada de Laplace e pela decomposição de Adomian.
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